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Funding statement
G.D. Egbert, N.M. Meqbel and A. Kelbert were supported
by NSF grant EAR1053628, and DOE grant DE-FG02-06ER15819.
P.E. Wannamaker was funded by NSF grant EAR08-43725 under the EarthScope program. A. Schultz was supported by Incorporated Research Institutions for Seismology (IRIS) subcontract
75-MT, under National Science Foundation Cooperative Agreement
No. EAR-0733069. Data from the TA network are made freely
available as part of the EarthScope USArray facility (http://www.earthscope.org), operated by Incorporated Research Institutions for Seismology (IRIS) and supported by the National Science Foundation, under Cooperative Agreements EAR-0323309, EAR-0323311,
EAR-0733069. The main inversion results were accomplished using computation resources of the GFZ German Research Centre for Geosciences, Potsdam.
Remove constraint Funding statement: G.D. Egbert, N.M. Meqbel and A. Kelbert were supported
by NSF grant EAR1053628, and DOE grant DE-FG02-06ER15819.
P.E. Wannamaker was funded by NSF grant EAR08-43725 under the EarthScope program. A. Schultz was supported by Incorporated Research Institutions for Seismology (IRIS) subcontract
75-MT, under National Science Foundation Cooperative Agreement
No. EAR-0733069. Data from the TA network are made freely
available as part of the EarthScope USArray facility (http://www.earthscope.org), operated by Incorporated Research Institutions for Seismology (IRIS) and supported by the National Science Foundation, under Cooperative Agreements EAR-0323309, EAR-0323311,
EAR-0733069. The main inversion results were accomplished using computation resources of the GFZ German Research Centre for Geosciences, Potsdam.